Moving from the upper course of a river to the lower course effects the rates of erosion, transportation and deposition change. This results in the development of large and small scale landforms.
The river picks up sediment and carries it downstream in different ways.
There are four types of transportation:
Traction – large, heavy pebbles are rolled along the river bed. This is most common near the sourceThe place where a river starts in its upper course. of a river, as here the load is larger.
Saltation – pebbles are bounced along the river bed, most commonly near the source.
Suspension – lighter sediment is suspended (carried) within the water, most commonly near the mouthThe place where a river meets the sea. of the river.
Solution – the transport of dissolved chemicals. This varies along the river depending on the presence of soluble rocks.